Classification Of Metamorphic
Rocks
Ø Metamorphic
rocks have been variously classified on the basis of texture and structure,
degree of metamorphism, mineralogical composition and mode of origin etc.
Ø A very
general two-fold classification based on the presence or absence of layered
structure or
FOLIATION as defined above is as follows:
(a) Foliated
Rocks
Ø All
metamorphic rocks showing development of conspicuous parallelism in their
mineralogical and structural constitution falling under the general term
foliation are grouped together as foliated rocks.
Ø The
parallelism indicating features include slaty cleavage, schistosity and
gneissose structures
Ø
Typical rocks included in this group are slates,
phyllites, schists and gneisses of great variety.
(b)Non-Foliated
Rocks
Ø
Included in this group are all those metamorphic rocks characterised with total
or nearly total absence of foliation or parallelism of mineralogicaJ
constituents.
Ø Typical examples of non-foliated rocks are
quartzites, hornfels, marbles, amphibolites and soapstone etc.
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